標(biāo)題: Titlebook: Breaking Waves; IUTAM Symposium Sydn Michael L. Banner,Roger H. J. Grimshaw Conference proceedings 1992 Springer-Verlag, Berlin Heidelberg [打印本頁] 作者: bile-acids 時(shí)間: 2025-3-21 18:24
書目名稱Breaking Waves影響因子(影響力)
書目名稱Breaking Waves影響因子(影響力)學(xué)科排名
書目名稱Breaking Waves網(wǎng)絡(luò)公開度
書目名稱Breaking Waves網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Breaking Waves被引頻次
書目名稱Breaking Waves被引頻次學(xué)科排名
書目名稱Breaking Waves年度引用
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書目名稱Breaking Waves讀者反饋
書目名稱Breaking Waves讀者反饋學(xué)科排名
作者: facetious 時(shí)間: 2025-3-21 21:47
Capillary Rollers and Boresme phase speed. The dynamical theory of the generation of parasitic capillaries has been developed by Longuet-Higgins (1963), Crapper (1970) and Ruvinsky et al. (1981, 1985, 1991). This so far takes into account only the first-order effects of viscous damping.作者: incisive 時(shí)間: 2025-3-22 01:55
Effect of Breaking Waves on the Transport of Heat and Vapor Fluxes from the Oceanstent heat from the ocean. Field data reduced by the present model gives highly consistent results. During high-sea states, the vertical energy flux from the ocean was found to be more than four times larger than the existing formulation, in which the effect of water droplets was not taken into consideration.作者: PANT 時(shí)間: 2025-3-22 04:54 作者: dissent 時(shí)間: 2025-3-22 09:45 作者: fabricate 時(shí)間: 2025-3-22 16:21 作者: 香料 時(shí)間: 2025-3-22 18:34 作者: Obstacle 時(shí)間: 2025-3-22 22:54 作者: INCUR 時(shí)間: 2025-3-23 03:29 作者: 揭穿真相 時(shí)間: 2025-3-23 09:17 作者: 強(qiáng)所 時(shí)間: 2025-3-23 13:47
Breaking Wave Statistics Obtained During ‘Swade’published field measurements of breaking wave statistics, using different techniques, can be encompassed nicely by the present void fraction statistics in a more meaningful and orderly way. The frequency, or number fraction, of breaking waves levels off as the wind speed increases.作者: Magnificent 時(shí)間: 2025-3-23 15:50
Conference proceedings 1992 technological importance, A familiar illustration is provided with white-capping and microbreaking of the wind-driven ocean sUrface waves, which is believed to play an important part in the transfers of momentum, mass and heat across the air-sea interface, as well as in the production of underwater作者: DALLY 時(shí)間: 2025-3-23 18:15
Reporting Standards for Literature Reviewsrgy transfer between the waves in the equilibrium range and those at the spectral peak, involving both upward and downward cascading of the wave energy. The variation of z. directly reflects the degree of over- and under-saturation of the level of the equilibrium range.作者: 辯論的終結(jié) 時(shí)間: 2025-3-24 01:54 作者: 平 時(shí)間: 2025-3-24 02:32
https://doi.org/10.1007/978-1-4614-1545-9o intensive observational scrutiny. These include: changes in microwave reflectivity; stress and gas transfer enhancement; formation of bubble clouds and sound generation; dissipation of surface waves.作者: GOUGE 時(shí)間: 2025-3-24 08:47
Plural Identities in the Age of Nationalismsme phase speed. The dynamical theory of the generation of parasitic capillaries has been developed by Longuet-Higgins (1963), Crapper (1970) and Ruvinsky et al. (1981, 1985, 1991). This so far takes into account only the first-order effects of viscous damping.作者: 性冷淡 時(shí)間: 2025-3-24 11:05 作者: 偏見 時(shí)間: 2025-3-24 17:37 作者: 領(lǐng)袖氣質(zhì) 時(shí)間: 2025-3-24 20:36
The Physical Consequences of Wave Breaking in Deep Waterion on the ocean surface. In particular, the complex process of wave breaking has a wide range of consequences for remote sensing, momentum, heat and mass transfer and oceanic acoustics. In this paper we consider some of the more important effects of wave breaking that have recently been subjected t作者: 下邊深陷 時(shí)間: 2025-3-25 02:20
Capillary Rollers and Bores the forward face of moderately short gravity waves, especially those with wavelengths 5 to 50 cm; see Figure la. These capillary waves were first studied experimentally by Cox (1958). Evidently their existence depends on the fact that a gravity wave and a much shorter capillary wave may have the sa作者: hemorrhage 時(shí)間: 2025-3-25 04:51 作者: dragon 時(shí)間: 2025-3-25 08:47 作者: 為寵愛 時(shí)間: 2025-3-25 13:06
Observations of the Enhancement of Kinetic Energy Dissipation Beneath Breaking Wind Wavesonal to the cube of the friction velocity .. and inversely proportional to depth, ∈αu...With a concomitant logarithmic velocity profile, this is consistent with a total kinetic energy flux from the wind of . . However, in fully rough flow and strongly forced waves the energy input may be one to two 作者: 沖擊力 時(shí)間: 2025-3-25 19:18
Microwave Backscattering from Laboratory Wind-Wave Surfaces and its Relation to Wave Breaking with Bnsity of the backscattered signature is in phase with the surface displacement. Variation of the Doppler velocity also corresponds to the phase of the individual waves. High Doppler velocity observed at the crests of the individual waves coincides with the propagating speed of the crests. It is conc作者: 詼諧 時(shí)間: 2025-3-25 20:46 作者: LAP 時(shí)間: 2025-3-26 03:25 作者: 2否定 時(shí)間: 2025-3-26 05:35
Sound Production and Air Entrainment by Breaking Waves: A Review of Recent Laboratory Experimentscatter from individual breaking events are found to correlate with the important kinematic and dynamic properties of the breaking waves. Air entrainment measurements show that the bubble plume characteristics evolve as simple functions of time. A large fraction (30% to 50%) of the surface wave energ作者: Relinquish 時(shí)間: 2025-3-26 10:18
Wave Breaking in the Presence of Wind Drift and Opposed Swellopagating against the wind. It is shown that the growth of the wind waves is much intensified by swell propagating against the wind, when the swell steepness increases. This phenomenon shows clear contrast to the attenuation of the wind waves by swell propagating in the direction of the wind. Anothe作者: 說不出 時(shí)間: 2025-3-26 14:20 作者: CLEFT 時(shí)間: 2025-3-26 17:15 作者: seduce 時(shí)間: 2025-3-27 00:29 作者: NEEDY 時(shí)間: 2025-3-27 01:51
Possible Mechanisms for Wave Breaking, by the dominant ones. We seek confirmation for this in the analysis of accurate wave records taken from an oceanographic platform in the Adriatic. Consistently with the forementioned mechanism, we find evidence of grouping of short waves just ahead of the dominant crests in the active wind cases, 作者: BROOK 時(shí)間: 2025-3-27 06:21
Plural Identities in the Age of Nationalismsnd . is a characteristic wind velocity. The other spectrum corresponds to an inverse cascade of energy in which wavelengths increase (“wave aging”) (Zakharov and Zaslavsky, 1981). It is realized at ω< ω.. The inverse cascade leads to the production of “aged waves” that are common in an open ocean (G作者: 圓木可阻礙 時(shí)間: 2025-3-27 12:55
Making Knowledge Management Clickable to wall layer scaling. In the intermediate region the dissipation decays more rapidly than z.. This may be viewed as a transition region between the deeper shear layer and the near surface region, with intense patches of breaking-imposed turbulence. In the absence of density stratification, dissipa作者: Spartan 時(shí)間: 2025-3-27 14:29 作者: 和平主義 時(shí)間: 2025-3-27 21:41
Leisure workshops for parents and carersetween the upper and lower sidebands but with the onset of breaking a smaller fraction of the initial energy was transferred to the upper sideband. The spectral behaviour of these evolving wave packets shows a number of features in common with that of wind waves observed in the open sea.作者: left-ventricle 時(shí)間: 2025-3-28 01:25 作者: 節(jié)約 時(shí)間: 2025-3-28 02:45 作者: Amorous 時(shí)間: 2025-3-28 07:08
Dependence of Wave-Breaking Statistics on Wind Stress and Wave Developmentcombination of.. and ../.. can be understood in physical terms. Furthermore, for the larger values of .. the dependence of wave breaking on wave age was stronger than at the low end of the values for .. and ../... Thus, both the level of wave development as determined by inverse wave age, which we m作者: 付出 時(shí)間: 2025-3-28 14:05
The Sideband Instability and the Onset of Wave Breakingetween the upper and lower sidebands but with the onset of breaking a smaller fraction of the initial energy was transferred to the upper sideband. The spectral behaviour of these evolving wave packets shows a number of features in common with that of wind waves observed in the open sea.作者: 開始從未 時(shí)間: 2025-3-28 17:03 作者: 廢墟 時(shí)間: 2025-3-28 21:05 作者: 苦笑 時(shí)間: 2025-3-29 02:14 作者: Horizon 時(shí)間: 2025-3-29 03:54
Mechanisms of Water-Wave Breakingwards breaking or the effects of breaking. As well as plunging and spilling breakers other less usual topics are considered including examples where the free surface “breaks” at a trough rather than a crest.作者: BLUSH 時(shí)間: 2025-3-29 10:15
Possible Mechanisms for Wave Breaking, by the dominant ones. We seek confirmation for this in the analysis of accurate wave records taken from an oceanographic platform in the Adriatic. Consistently with the forementioned mechanism, we find evidence of grouping of short waves just ahead of the dominant crests in the active wind cases, while no grouping is found in the case of swell.作者: Ceramic 時(shí)間: 2025-3-29 13:54
Individual Liberties and Community Tieswards breaking or the effects of breaking. As well as plunging and spilling breakers other less usual topics are considered including examples where the free surface “breaks” at a trough rather than a crest.作者: 光明正大 時(shí)間: 2025-3-29 15:42 作者: 抱怨 時(shí)間: 2025-3-29 20:23
Plural Identities in the Age of NationalismsSurf zone dynamics is a highly complicated topic in hydrodynamics which deals with the waves and wave generated phenomena in the region between the breaker line on a beach and the shoreline.作者: 無聊的人 時(shí)間: 2025-3-30 01:04 作者: left-ventricle 時(shí)間: 2025-3-30 06:43 作者: 自傳 時(shí)間: 2025-3-30 11:11
Acoustical Measurement of Breaking Surfaces WavesBreaking surface waves can be detected acoustically in the open ocean with a small hydrophone array. We describe the technique used for this purpose and show a few results, including measurement of breaking wave propagation speed and the characteristics of the acoustical radiation.作者: 粉筆 時(shí)間: 2025-3-30 13:17
https://doi.org/10.1007/978-1-4614-1545-9ion on the ocean surface. In particular, the complex process of wave breaking has a wide range of consequences for remote sensing, momentum, heat and mass transfer and oceanic acoustics. In this paper we consider some of the more important effects of wave breaking that have recently been subjected t作者: GRATE 時(shí)間: 2025-3-30 18:16 作者: 紅潤(rùn) 時(shí)間: 2025-3-30 21:04 作者: 暗語 時(shí)間: 2025-3-31 01:53
Plural Identities in the Age of Nationalisms density to water density provides a small parameter, with the consequence that characteristic wave amplitudes in typical situations are small. This justifies “a weak turbulent”approach to the problem of a statistical description, using an expansion in powers of nonlinearity..The simplest variant of作者: 無王時(shí)期, 時(shí)間: 2025-3-31 08:07
Making Knowledge Management Clickableonal to the cube of the friction velocity .. and inversely proportional to depth, ∈αu...With a concomitant logarithmic velocity profile, this is consistent with a total kinetic energy flux from the wind of . . However, in fully rough flow and strongly forced waves the energy input may be one to two 作者: Circumscribe 時(shí)間: 2025-3-31 10:50
Data Catalogs and Governance Toolsnsity of the backscattered signature is in phase with the surface displacement. Variation of the Doppler velocity also corresponds to the phase of the individual waves. High Doppler velocity observed at the crests of the individual waves coincides with the propagating speed of the crests. It is conc作者: GIBE 時(shí)間: 2025-3-31 14:20 作者: FLAIL 時(shí)間: 2025-3-31 19:57
https://doi.org/10.1007/978-1-4899-4487-0 drag objects for the wind. The resultant transport equations for the momentum, temperature, humidity, and micro-water droplets fields are treated as inter-coupled fields. In this study, we have found that the micro droplets produced by breaking waves is a major source of atmospheric moisture and la作者: Comedienne 時(shí)間: 2025-3-31 22:49 作者: 啤酒 時(shí)間: 2025-4-1 05:53
https://doi.org/10.1007/978-1-4899-4487-0opagating against the wind. It is shown that the growth of the wind waves is much intensified by swell propagating against the wind, when the swell steepness increases. This phenomenon shows clear contrast to the attenuation of the wind waves by swell propagating in the direction of the wind. Anothe作者: 兇兆 時(shí)間: 2025-4-1 06:31 作者: custody 時(shí)間: 2025-4-1 10:28
Rob Dekkers,Lindsey Carey,Peter Langhornelue measured during SWADE (Weller, et. al, 1991) with the wind speed up to 15 m/s and gusts to 18 m/s is about 60%. The duration for the void fraction event is about, on average, 0.5 sec at the depth of 12″ for the average wave period of about 5.5 sec. Much less void fraction is observed below 24″. 作者: Madrigal 時(shí)間: 2025-4-1 15:10
Reporting Standards for Literature Reviewseaking should play an essential role. A 4.5-hour time series of wind profile and wind-wave statistics, obtained at an oceanographic tower station under a winter monsoon wind, were reanalyzed. The main part of the equilibrium range of wind-wave spectra always follows the σ.-slope, though the energy l
